Rapid light carbon releases and increased aridity linked to Karoo–Ferrar magmatism during the early Toarcian oceanic anoxic event

Large-scale release of isotopically light carbon is responsible for the carbon isotope excursion (CIE) of the Toarcian Oceanic Anoxic Event during the Lower Jurassic. Proposed sources include methane hydrate dissociation, volcanogenic outgassing of carbon dioxide and/or thermogenic methane release f...

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Detalles Bibliográficos
Autores principales: Font, Eric, Duarte, Luís Vítor, Dekkers, Mark J., Remazeilles, Celine, Egli, Ramon, Spangenberg, Jorge E., Fantasia, Alicia, Ribeiro, Joana, Gomes, Elsa, Mirão, José, Adatte, Thierry
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2022
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8921222/
https://www.ncbi.nlm.nih.gov/pubmed/35288615
http://dx.doi.org/10.1038/s41598-022-08269-y

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8921222/
https://www.ncbi.nlm.nih.gov/pubmed/35288615
http://dx.doi.org/10.1038/s41598-022-08269-y

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